Geomorphological constraining of tsunami (?) run-up in the Alcantarilha coastal lowland (Central Algarve, Portugal)

The Alcantarilha lowland, partly barred by a well developed barrier, including foredunes covering Pleistocene-Holocene beachrock and aeolianite, develops across the Alcantarilha infilled estuary, the beach-dune extending further SE until the Salgados lagoon. A topographic and coring survey revealed...

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Bibliographic Details
Main Author: Dinis, Jorge (author)
Other Authors: Andrade, César (author), Oliveira, Alexandre (author), Freitas, Maria (author), Cunha, Pedro (author), Martins, António (author), Costa, Pedro (author)
Format: article
Language:por
Published: 2016
Subjects:
Tsunami run up
Alcantarilha coastal
Algarve
trenches
Online Access:http://hdl.handle.net/10174/18476
Country:Portugal
Oai:oai:dspace.uevora.pt:10174/18476

Internet

http://hdl.handle.net/10174/18476

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